Paul. J. Crutzen received the Nobel Prize in Chemistry with Mario J. Molina and F. Sherwood Rowland in 1995.He has triggered global policy debates on nuclear winter, Anthropocene and sustainability.

• The Background of an Ozone Researcher: A BriefAutobiography.- Complete Bibliography of the Writings of Paul J. Crutzen (1965-2014).- TheInfluence ofNitrogen Oxides on Atmospheric Ozone Content.- Biomass Burning as a Source ofAtmospheric Gases CO2, H2, N2O, NO, CH3Cland COS.- The Atmosphere after a Nuclear War:Twilight at Noon.- Nitric–acidCloud Formation in the Cold Antarctic Stratosphere – A Major Cause for theSpringtime Ozone Hole.- Biomass Burning in the Tropics: Impact on Atmospheric Chemistry andBiogeochemical Cycles.- A Mechanism for Halogen Release from Sea-saltAerosol in the Remote Marine Boundary Layer.

Paul. J. Crutzen received the Nobel Prize in Chemistry with Mario J. Molina and F. Sherwood Rowland in 1995.He has triggered global policy debates on nuclear winter, Anthropocene and sustainability.

• The Background of an Ozone Researcher: A BriefAutobiography.- Complete Bibliography of the Writings of Paul J. Crutzen (1965-2014).- TheInfluence ofNitrogen Oxides on Atmospheric Ozone Content.- Biomass Burning as a Source ofAtmospheric Gases CO2, H2, N2O, NO, CH3Cland COS.- The Atmosphere after a Nuclear War:Twilight at Noon.- Nitric–acidCloud Formation in the Cold Antarctic Stratosphere – A Major Cause for theSpringtime Ozone Hole.- Biomass Burning in the Tropics: Impact on Atmospheric Chemistry andBiogeochemical Cycles.- A Mechanism for Halogen Release from Sea-saltAerosol in the Remote Marine Boundary Layer.

Paul. J. Crutzen received the Nobel Prize in Chemistry with Mario J. Molina and F. Sherwood Rowland in 1995.He has triggered global policy debates on nuclear winter, Anthropocene and sustainability.

• The Background of an Ozone Researcher: A BriefAutobiography.- Complete Bibliography of the Writings of Paul J. Crutzen (1965-2014).- TheInfluence ofNitrogen Oxides on Atmospheric Ozone Content.- Biomass Burning as a Source ofAtmospheric Gases CO2, H2, N2O, NO, CH3Cland COS.- The Atmosphere after a Nuclear War:Twilight at Noon.- Nitric–acidCloud Formation in the Cold Antarctic Stratosphere – A Major Cause for theSpringtime Ozone Hole.- Biomass Burning in the Tropics: Impact on Atmospheric Chemistry andBiogeochemical Cycles.- A Mechanism for Halogen Release from Sea-saltAerosol in the Remote Marine Boundary Layer.